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USGS · fs22295

Reversal of declining ground-water levels in the Chicago area

Abstract

Abundant water resources have been an important part of the economic development of the Chicago area for more than a century. The city of Chicago, Ill., and other lakefront towns have used Lake Michigan as a water supply. Where water from Lake Michigan was not available or a need for supplemental water supplies was present, deep wells (generally greater than 700 feet) provided a clean, reliable, and abundant water supply from the Cambrian-Ordovician aquifer. Public water suppliers withdraw the most ground water in the eight-county Chicago area (Cook, Du Page, Grundy, Kane, Kendall, Lake, McHenry, and Will Counties). This report describes a reversal in the trend of declining ground-water levels in the Cambrian-Ordovician aquifer in the Chicago area as public water suppliers have converted from the withdrawal of ground water from wells to the withdrawal of surface water from Lake Michigan.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 41.7180304600481° to 42.06968462804663° latitude; -87.9510498046875° to -87.5445556640625° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Charles Avery. 1995. Reversal of declining ground-water levels in the Chicago area. https://doi.org/10.3133/fs22295

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